Titlebook: Landform - Structure, Evolution, Process Control; Proceedings of the I Jan-Christoph Otto,Richard Dikau Conference proceedings 2010 Springe

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,Hydrological Analyses as a Prerequisite for Soil Erosion Modeling – Landscape Related Studies in a conducted with the WaSiM-ETH model. The model was calibrated for 1999 and successfully validated for 2000 using observed runoff data (Pearson’s . = 0.9 for both years). The validated model was used to compute spatial and temporal differentiated soil moisture as an essential prerequisite for event-ba

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Patterns of Multiannual Aggradation of Permafrost in Rock Walls with and Without Hydraulic Interconsized, that interconnective systems with cleft water percolation from glacierets close to 0°C are high-entropy systems that balance rock masses at 0°C and prevent cooling but are not effective in excessive melting, as thermal conduction away from water pathways into compact rock is a function of sen

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Resilience, Integrity and Ecosystem Dynamics: Bridging Ecosystem Theory and Management, into two separate sequences, a complexifying phase which is characterized by orientor optimization and a destruction based phase which follows disturbances. The two developmental pathways are integrated in a modified illustration of the “adaptive cycle”. Based on these fundamentals, the recent defi

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